Episodes 2003; 26(3): 235-238
Published online September 1, 2003
https://doi.org/10.18814/epiiugs/2003/v26i3/014
Copyright © International Union of Geological Sciences.
Lisetta Giacomelli1, Annamaria Perrotta2, Roberto Scandone3, Claudio Scarpati2
1Gruppo Nazionale di Vulcanologia, Via Nizza 128, 00193 Roma, Italy.
2Dipartimento di Geofisica e Vulcanologia, Largo San Marcellino 10, 80138, Napoli, Italy.
3Dipartimento di Fisica, Università di Roma Tre, 00146, Roma, Italy
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The eruption of Vesuvius of 79 AD caused extensive destructions all over the Campanian area, engulfing the cities of Pompeii, Herculaneum, Oplonti and Stabiae. The eruption followed a long quiescence period and the inhabitants of the area were surprised by the volcanic events. The first part of the eruption was characterized by a widespread dispersal of pumices from a high eruptive column. The second part of the eruption, characterized by pyroclastic flows emplacement, caused the major damages with extensive life losses in most of the towns surrounding the volcano. In Pompeii, the major casualties during the first phase resulted from roof collapses; during the second phase, people were killed either by physical trauma due to the kinetic energy of the flow or by suffucation because of the ash-rich atmosphere.